For the ΔDEC case, the summer snowfall shows a weaker, but qualitatively identical behavior for Kunlun Shan and Pamir, and the increase in summer snowfall is highly significant ( P ≪ 0.01) when aggregated over the region, with a mean increase of summer snowfall of 2 and 5%, respectively.
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Irrigation as a Potential Driver for Anomalous Glacier Behavior in High Mountain Asia.
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